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Department of Geology

Our mission is to pursue excellence in fundamental and applied research in the earth sciences, sustain quality in graduate education, and provide outreach and service for the benefit of society and the environment.

The Department is committed to maintain a diversity of specialties to provide broad-based graduate curriculum in the Geosciences. We value all our core programs and will take advantage of special initiatives that fit with our mission to upgrade those programs as opportunities arise.

# Title Research Year
791 Ground magnetic survey on some basaltic bodies in Gebal Gebeil and west of El-Bahnasa areas, Western desert, Egypt. 2003
792 Palaeoecological Significance of Pteridophyte-Arucaroid Acme in the Lower Cretaceous Sequence of the Siqeifa 1-x Borehole, north Western Egypt 2003
793 Sedimentological approach to high resolution Sequence Stratigraphy of the Upper Cretaceous-Eocene Successions, Farafra Oasis, Western Desert, Egypt. 2003
794 Kinematics of conjugate Riedel shear zone systems in the area of Gebel El Mayyit , Central Eastern Desert, Egypt. 2003
795 Upper Paleocene-lower Eocene Planktonic foraminiferal biostratigraphy of the Dababiya section, Upper Nile Valley (Egypt). In: Ouda, Kh., and Aubry, M.-P., Eds. 2003
796 Upper Paleocene-lower Eocene planktonic foraminiferal biostratigraphy of the Wadi Abu Ghurra section, Upper Nile Valley (Egypt)‏
2003
797 Pre-Orogenic Magmatic Phases of Baranis Area, Southeastern Desert, Egypt. 2003
798 Yossef, M.M., Hassan, M.A. and Saber M. (2003): Tectonic evolution and deformation phases of the area around Gebel El-Mayyit, Central Eastern Desert, Egypt. Proceeding of Thrid International Conference on the Geology of Africa. Assiut Univ. Egypt. 1: 173- 2003
799 Integrated biostratigraphy of the Coniacian – Santonian Sequence, southwestern Sinai, Egypt. 2002
800 DIFFERENT GEOTHERMOBAROMETRIC MODELS OF COEXISTING GARNET-BIOTITE, GARNET-PLAGIOCLASE AND ALKALI FELDSPAR-PLAGIOCLASE FROM DIFFERENT LOCALITIES IN THE CENTRAL EASTERN DESERT, EGYPT. 2002